mantle drag
Quick Summary
Mantle drag refers to the resistance encountered by tectonic plates as they move across the Earth's mantle. This movement is primarily driven by convection currents within the mantle, fueled by heat from radioactive decay.12
While convection is the main driver, other forces contribute:
* Slab pull: The weight of a dense oceanic plate sinking at a subduction zone pulls the rest of the plate along.21
* Ridge push: Gravitational force at higher-elevation mid-ocean ridges pushes plates away as they cool and become denser.21
Mantle drag itself can influence plate speed, but the exact relationship between mantle flow and surface plate movement is still a subject of ongoing research. Seismic tomography helps visualize these deep Earth processes by creating images of the mantle's interior.23
Ask Britannica AI about this topic
Britannica doesn't have a full article on this topic, so we've curated a list of our relevant coverage.
